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      The future of the northeast Atlantic benthic flora in a high CO 2 world

      review-article
      1 , 1 , 2 , 3 , 4 , 5 , 3 , 6 , 3 , 7 , 1 , 8 , 9 , 10 , 3 , 11 , 12 , 13 , 14 , 5 , 15 , 16 , 17 , 18 , 19 , 20 , 21 , 22 ,   20 , 7 , 23 , 16
      Ecology and Evolution
      BlackWell Publishing Ltd
      Calcified algae, climate change, invasive species, macroalgae, microphytobenthos, seagrasses, volatile gases

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          Abstract

          Seaweed and seagrass communities in the northeast Atlantic have been profoundly impacted by humans, and the rate of change is accelerating rapidly due to runaway CO 2 emissions and mounting pressures on coastlines associated with human population growth and increased consumption of finite resources. Here, we predict how rapid warming and acidification are likely to affect benthic flora and coastal ecosystems of the northeast Atlantic in this century, based on global evidence from the literature as interpreted by the collective knowledge of the authorship. We predict that warming will kill off kelp forests in the south and that ocean acidification will remove maerl habitat in the north. Seagrasses will proliferate, and associated epiphytes switch from calcified algae to diatoms and filamentous species. Invasive species will thrive in niches liberated by loss of native species and spread via exponential development of artificial marine structures. Combined impacts of seawater warming, ocean acidification, and increased storminess may replace structurally diverse seaweed canopies, with associated calcified and noncalcified flora, with simple habitats dominated by noncalcified, turf-forming seaweeds.

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          Most cited references185

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          Impacts of ocean acidification on marine organisms: quantifying sensitivities and interaction with warming

          Ocean acidification represents a threat to marine species worldwide, and forecasting the ecological impacts of acidification is a high priority for science, management, and policy. As research on the topic expands at an exponential rate, a comprehensive understanding of the variability in organisms' responses and corresponding levels of certainty is necessary to forecast the ecological effects. Here, we perform the most comprehensive meta-analysis to date by synthesizing the results of 228 studies examining biological responses to ocean acidification. The results reveal decreased survival, calcification, growth, development and abundance in response to acidification when the broad range of marine organisms is pooled together. However, the magnitude of these responses varies among taxonomic groups, suggesting there is some predictable trait-based variation in sensitivity, despite the investigation of approximately 100 new species in recent research. The results also reveal an enhanced sensitivity of mollusk larvae, but suggest that an enhanced sensitivity of early life history stages is not universal across all taxonomic groups. In addition, the variability in species' responses is enhanced when they are exposed to acidification in multi-species assemblages, suggesting that it is important to consider indirect effects and exercise caution when forecasting abundance patterns from single-species laboratory experiments. Furthermore, the results suggest that other factors, such as nutritional status or source population, could cause substantial variation in organisms' responses. Last, the results highlight a trend towards enhanced sensitivity to acidification when taxa are concurrently exposed to elevated seawater temperature.
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            Evidence for upwelling of corrosive "acidified" water onto the continental shelf.

            The absorption of atmospheric carbon dioxide (CO2) into the ocean lowers the pH of the waters. This so-called ocean acidification could have important consequences for marine ecosystems. To better understand the extent of this ocean acidification in coastal waters, we conducted hydrographic surveys along the continental shelf of western North America from central Canada to northern Mexico. We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of approximately 40 to 120 meters along most transect lines and all the way to the surface on one transect off northern California. Although seasonal upwelling of the undersaturated waters onto the shelf is a natural phenomenon in this region, the ocean uptake of anthropogenic CO2 has increased the areal extent of the affected area.
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              Volcanic carbon dioxide vents show ecosystem effects of ocean acidification.

              The atmospheric partial pressure of carbon dioxide (p(CO(2))) will almost certainly be double that of pre-industrial levels by 2100 and will be considerably higher than at any time during the past few million years. The oceans are a principal sink for anthropogenic CO(2) where it is estimated to have caused a 30% increase in the concentration of H(+) in ocean surface waters since the early 1900s and may lead to a drop in seawater pH of up to 0.5 units by 2100 (refs 2, 3). Our understanding of how increased ocean acidity may affect marine ecosystems is at present very limited as almost all studies have been in vitro, short-term, rapid perturbation experiments on isolated elements of the ecosystem. Here we show the effects of acidification on benthic ecosystems at shallow coastal sites where volcanic CO(2) vents lower the pH of the water column. Along gradients of normal pH (8.1-8.2) to lowered pH (mean 7.8-7.9, minimum 7.4-7.5), typical rocky shore communities with abundant calcareous organisms shifted to communities lacking scleractinian corals with significant reductions in sea urchin and coralline algal abundance. To our knowledge, this is the first ecosystem-scale validation of predictions that these important groups of organisms are susceptible to elevated amounts of p(CO(2)). Sea-grass production was highest in an area at mean pH 7.6 (1,827 (mu)atm p(CO(2))) where coralline algal biomass was significantly reduced and gastropod shells were dissolving due to periods of carbonate sub-saturation. The species populating the vent sites comprise a suite of organisms that are resilient to naturally high concentrations of p(CO(2)) and indicate that ocean acidification may benefit highly invasive non-native algal species. Our results provide the first in situ insights into how shallow water marine communities might change when susceptible organisms are removed owing to ocean acidification.
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                Author and article information

                Journal
                Ecol Evol
                Ecol Evol
                ece3
                Ecology and Evolution
                BlackWell Publishing Ltd (Oxford, UK )
                2045-7758
                2045-7758
                July 2014
                18 June 2014
                : 4
                : 13
                : 2787-2798
                Affiliations
                [1 ]Department of Life Sciences, The Natural History Museum Cromwell Road, London, SW7 5BD, UK
                [2 ]School of Earth and Ocean Sciences, Cardiff University Main Building, Park Place, Cardiff, CF10 3YE, UK
                [3 ]Marine Biological Association of the UK Citadel Hill, Plymouth, PL1 2PB, UK
                [4 ]Ocean and Earth Science, National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
                [5 ]School of Geographical and Earth Sciences, University of Glasgow Glasgow, G12 8QQ, UK
                [6 ]Marine Plant Ecology Research Group (ALGAE), Centre of Marine Sciences (CCMAR), University of Algarve Campus of Gambelas, Faro, 8005-139, Portugal
                [7 ]School of Biological Sciences, University of Essex Colchester, CO4 3SQ, UK
                [8 ]Institute of Zoology, Zoological Society of London Regent's Park, London, NW1 4RY, UK
                [9 ]Department of Zoology, The University of British Columbia #4200-6270 University Blvd., Vancouver, British Columbia, V6T 1Z4, Canada
                [10 ]DiSTAV - University of Genoa C.so Europa 26, Genoa, 16132, Italy
                [11 ]Department of Earth and Environmental Sciences, University of St Andrews St Andrews, Fife, KY16 9AL, UK
                [12 ]Scottish Oceans Institute, University of St Andrews St Andrews, Fife, KY16 8LB, UK
                [13 ]Scottish Marine Institute Oban, Argyll, PA37 1QA, UK
                [14 ]Institute of Evolutionary Biology, University of Edinburgh The King's Building, West Mains Road, Edinburgh, EH9 3JT, UK
                [15 ]Institute of Biology, Environmental and Rural Sciences, Aberystwyth University Aberystwyth, UK
                [16 ]Marine Biology and Ecology Research Centre, School of Marine Sciences and Engineering, Plymouth University PL4 8AA, UK
                [17 ]CNRS, UMR 7144, Station Biologique de Roscoff, Place Georges Teissier, Roscoff Cedex, 29688, France
                [18 ]UPMC Univ. Paris 6, UMR 7144 Station Biologique de Roscoff, Place Georges Teissier, Roscoff Cedex, 29688, France
                [19 ]Plymouth Marine Laboratory Prospect Place, The Hoe, Plymouth, PL1 3DH, UK
                [20 ]School of Earth Sciences, University of Bristol Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, UK
                [21 ]Division of Plant Science, University of Dundee at the James Hutton Institute Invergowrie, Dundee, DD2 5DA, UK
                [22 ]Plant Functional Biology and Climate Change Cluster, University of Technology Sydney Ultimo, NSW 2007, Australia
                [23 ]Leibniz-Zentrum für Marine Tropenökologie Fahrenheitstraße 6, Bremen, D-28359, Germany
                Author notes
                Juliet Brodie, Department of Life Sciences, The Natural History Museum, Cromwell Road, London, SW7 5BD, UK. Tel: +44 207 942 5910; E-mail: j.brodie@ 123456nhm.ac.uk

                Funding Information This work was funded by the UK Ocean Acidification Research Programme (co-funded by NERC, Defra and DECC), NERC OARP Grant: NE/H016996/1 “Ocean Acidification Impacts on Sea-Surface Biogeochemistry and climate”.

                Article
                10.1002/ece3.1105
                4113300
                25077027
                60ec3ccd-aa31-4ca3-9b61-7afc5eacf4c1
                © 2014 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd.

                This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

                History
                : 31 January 2014
                : 15 April 2014
                : 22 April 2014
                Categories
                Review

                Evolutionary Biology
                calcified algae,climate change,invasive species,macroalgae,microphytobenthos,seagrasses,volatile gases

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